The Clearwater orogenic zone in central Idaho and W Montana contains at least 2 major NE-directed Cordilleran thrust plates of Early Proterozoic metasedimentary and metaigneous rocks that overrode previously folded Middle Proterozoic rocks of the Belt basin in Cretaceous time. The northeastward migration of the resultant thickened wedge of crustal material combined with Cretaceous subduction along the W continental margin produced a younger N Bitterroot lobe of the Idaho batholith relative to an older S Atlanta lobe. Eocene extensional unroofing and erosion of the Bitterroot lobe has exposed the roots of the thick Cordilleran thrust sheets.-Author
Citation Information
Publication Year | 1987 |
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Title | Basement thrust sheets in the Clearwater orogenic zone, central Idaho and western Montana ( USA). |
DOI | |
Authors | B. Skipp |
Publication Type | Article |
Publication Subtype | Journal Article |
Series Title | Geology |
Series Number | |
Index ID | 70014196 |
Record Source | USGS Publications Warehouse |
USGS Organization |